Lake Manitoba Water Qality & Ecosystem Health Workshop
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Origin of the Name Manitoba
On May 2, 1870, Sir John A. Macdonald The Origin of the Name The Narrows of Lake Manitoba (on PTH 68, 60 km west of the junction of announced that a new province was to enter Manitoba PTHs 6 and 68) Confederation under The Manitoba Act. He said the province’s name had been chosen for its pleasant sound and its associations with the The name Manitoba originated in the languages original inhabitants of the area. of the Aboriginal people who lived on the Prairies and travelled the waters of Lake Both the Cree and Assiniboin terms, and the Manitoba. legends and events associated with their use, are preserved forever in the name Manitoba. A These people, the Cree and Assiniboin First plaque commemorating its origin is located on Nations, introduced European explorers, traders the east side of the Lake Manitoba Narrows. and settlers to the region and its waterways. They also passed on to the newcomers the ancient names and poetic legends associated with the places they inhabited. More than two centuries of contact and trade between the Europeans and First Nations produced a blending of their languages. From Aboriginal name and legend to official title of the province, the evolution of the name Manitoba mirrors the history of the region. At the Lake Manitoba Narrows a strong wind can send waves washing against the limestone During the Red River Resistance of 1869-70, rocks of an offshore island. The unique sound Spence joined Louis Riel’s Métis Council. In from the waves is said to be the Manitou, or the spring of 1870, delegates from this council Great Spirit (in Ojibway, “Manito-bau”). -
Grand Rapids GS Short Term Extension Licence Request (2014
360 Portage Ave (16) Winnipeg Manitoba Canada R3C 0G8 Telephone / No de téléphone : 204-360-3018 Fax / No de télécopieur : 204-360-6136 [email protected] 2014 10 30 Mr. Rob Matthews Manager, Water Use Licensing Manitoba Conservation and Water Stewardship Box 16 - 200 Saulteaux Crescent Winnipeg MANITOBA R3J 3W3 Dear Mr. Matthews: GRAND RAPIDS WATER POWER SHORT-TERM EXTENSION LICENCE REQUEST We request a five year short-term extension licence for the Grand Rapids Generating Station under the provisions of Section 92(1) of Water Power Regulation 25/88R. We have included a Short Term Extension Report as supporting documentation and will continue to work with your Section to address this Water Power licence. Manitoba Hydro continues to operate the Grand Rapids Generating Station in accordance with the Final Licence issued on May 30, 1975 under the Water Power Act. The Final Licence expires on January 2, 2015. Manitoba Hydro requested a renewal licence on December 17, 2010. However, due to licensing requirements for other projects, Manitoba Hydro is requesting a short-term extension licence to allow the licence renewal to occur at a later date. Please call me at 204-360-3018 if you need additional information. Yours truly, pp: Brian Giesbrecht W.V. Penner, P. Eng. Manager Hydraulic Operations Department Encl. MJD/sl/ 00112-07311-0014_00 WATER POWER ACT LICENCES GRAND RAPIDS GENERATING STATION SHORT TERM LICENCE EXTENSION APPLICATION SUPPORTING DOCUMENTATION Prepared for: Manitoba Water Stewardship 200 Saulteaux Crescent Winnipeg MB R3J 3W3 Prepared by: Manitoba Hydro 360 Portage Avenue Winnipeg MB R3C 0G8 October 29, 2014 Report No: PS&O – 14/08 HYDRAULIC OPERATIONS DEPARTMENT POWER SALES & OPERATIONS DIVISION GENERATION OPERATIONS WATER POWER ACT LICENCES GRAND RAPIDS SHORT TERM LICENCE EXTENSION APPLICATION SUPPORTING DOCUMENTATION Originally signed by P.Chanel Originally signed by PREPARED BY: P.Chanel P. -
Wallace Mining and Mineral Prospects in Northern
r Geology V f .ibrary TN 27 7A3V/1 WALLACE MINING AND MINERAL PROSPECTS IN NORTHERN MANITOBA THE LIBRARY OF THE UNIVERSITY OF CALIFORNIA LOS ANGELES University of British Columbia D. REED LIBRARY The RALPH o DEPARTMENT OF GEOLOGY UNIVERSITY OF CALIFORNIA LOS ,-XGELES, CALIF. Northern Manitoba Bulletins Mining and Mineral Prospects in Northern Manitoba BY R. C. WALLACE PUBLISHED BY AUTHORITY OF GOVERNMENT OP MANITOBA OFFICE OF COMMISSIONER OF NORTHERN MANITOBA The Pas, Manitoba Northern Manitoba Bulletins Mining and Mineral Prospects in Northern Manitoba BY R. C. WALLACE PUBLISHED BY AUTHORITY OF GOVERNMENT OF MANITOBA OFFICE OF COMMISSIONER OF NORTHERN MANITOBA The Pas, Manitoba CONTENTS Chapter Page I. Introductory 5 II. Geological features ... 7 III. History of Mining Development 12 IV. Metallic Deposits: (A) Mineral belt north of The Pas .... 20 (1) Flin Flon and Schist Lake Districts. .... ....20 (2) Athapapuskow Lake District ..... ....27 (3) Copper and Brunne Lake Districts .....30 (4) Herb and Little Herb Lake Districts .... .....31 (5) Pipe Lake, Wintering Lake and Hudson Bay Railway District... 37 (B) Other mineral areas .... .....37 V. Non-metallic Deposits 38 (a) Structural materials 38 (ft) Fuels 38 (c) Other deposits. 39 VI. The Economic Situatior 40 VII. Bibliography 42 Appendix: Synopsis of Regulations governing the granting of mineral rights.. ..44 NORTHERN MANITOBA NORTHERN MANITOBA Geology Library INTRODUCTORY CHAPTER I. INTRODUCTORY Scope of Bulletin The purpose of this bulletin is to give a short description of the mineral deposits, in so far as they have been discovered and developed, in the territory which was added to the Province of Manitoba in the year 1912. -
Lithium Concentrations in Brine Springs Near Lake Winnipegosis
Lithium concentrations in brine springs near Lake Winnipego- GS2018-10 sis, west-central Manitoba (parts of NTS 63C, 62N16, 62O12, 13) 1 In Brief: by M.P.B. Nicolas and S.E. Grasby • Brine springs along Lake Winnipegosis contain low levels of lithium, averaging Summary 1263 ppb The most common and cost-effective source of lithium within the brine deposits • Goundwater mixing has diluted the lithium concen- are deep brines in continental sedimentary basins. Southern Manitoba has a complex tration coming out from the springs groundwater aquifer system, with salinities ranging from brines in the deeper aquifers • Deep subsurface Winnipeg and brine springs to freshwater in the shallower and eastern aquifers. The brine springs Formation brines have good potential as a lithium source occur along and near the shores of Lake Winnipegosis on large salt flats and have chemi- cal signatures indicative of mixed halite dissolution brine and freshwater. Lithium concen- trations in these brines range from 150 to 6300 ppb, with an average of 1263 ppb. Citation: Nicolas, M.P.B. and Grasby, S.E. 2018: Lithium concentra- Introduction tions in brine springs near Lake Saline groundwater in continental sedimentary basins are generated from evaporitic Winnipegosis, west-central Manitoba (parts of NTS 63C, concentration and/or halite dissolution, where the former is a primary process and the 62N16, 62O12, 13); in Report latter is a secondary (diagenetic) process (Clayton et al., 1966; Walter et al., 1990). Both of Activities 2018, Manitoba these mechanisms provide opportunities for trace elements to accumulate, potentially Growth, Enterprise and Trade, Manitoba Geological Survey, reaching economic concentrations. -
Geomorphic and Sedimentological History of the Central Lake Agassiz Basin
Electronic Capture, 2008 The PDF file from which this document was printed was generated by scanning an original copy of the publication. Because the capture method used was 'Searchable Image (Exact)', it was not possible to proofread the resulting file to remove errors resulting from the capture process. Users should therefore verify critical information in an original copy of the publication. Recommended citation: J.T. Teller, L.H. Thorleifson, G. Matile and W.C. Brisbin, 1996. Sedimentology, Geomorphology and History of the Central Lake Agassiz Basin Field Trip Guidebook B2; Geological Association of CanadalMineralogical Association of Canada Annual Meeting, Winnipeg, Manitoba, May 27-29, 1996. © 1996: This book, orportions ofit, may not be reproduced in any form without written permission ofthe Geological Association ofCanada, Winnipeg Section. Additional copies can be purchased from the Geological Association of Canada, Winnipeg Section. Details are given on the back cover. SEDIMENTOLOGY, GEOMORPHOLOGY, AND HISTORY OF THE CENTRAL LAKE AGASSIZ BASIN TABLE OF CONTENTS The Winnipeg Area 1 General Introduction to Lake Agassiz 4 DAY 1: Winnipeg to Delta Marsh Field Station 6 STOP 1: Delta Marsh Field Station. ...................... .. 10 DAY2: Delta Marsh Field Station to Brandon to Bruxelles, Return En Route to Next Stop 14 STOP 2: Campbell Beach Ridge at Arden 14 En Route to Next Stop 18 STOP 3: Distal Sediments of Assiniboine Fan-Delta 18 En Route to Next Stop 19 STOP 4: Flood Gravels at Head of Assiniboine Fan-Delta 24 En Route to Next Stop 24 STOP 5: Stott Buffalo Jump and Assiniboine Spillway - LUNCH 28 En Route to Next Stop 28 STOP 6: Spruce Woods 29 En Route to Next Stop 31 STOP 7: Bruxelles Glaciotectonic Cut 34 STOP 8: Pembina Spillway View 34 DAY 3: Delta Marsh Field Station to Latimer Gully to Winnipeg En Route to Next Stop 36 STOP 9: Distal Fan Sediment , 36 STOP 10: Valley Fill Sediments (Latimer Gully) 36 STOP 11: Deep Basin Landforms of Lake Agassiz 42 References Cited 49 Appendix "Review of Lake Agassiz history" (L.H. -
Faculty of Graduate Studies
3'A.C|IJL:IY 0F t'RA:)LlrÊ'TE Ë'TJIÏE'1 DEP/ìRTMfiÌT OF,- T],VJ ]. EI$GTIVEEBSNI] tilIÏVElRlrllty 03' j4AN:]"T0BA AN ÍN\TfißTTI.íTITTOJ\T O}' T}IE ÐTVERåJ.OIf C}:.rÎ NOR'IIìTB.N }4ANTTOEA I{ATE¡I.:3 J,NTO ].,AKE }IIAJü OÉA l- Jt t. .4. Fl:-¡40I{ n TI]Tfl:I:ì J:I{,PÅR]TÏAL FLI"LF],ffÆI\T 'sUBT\MTTEÐ CIF T'TIE REQLÍSAEME}Í?i3 iIÜR TTIE NEGBEE ÐF j/ÛslER Olr SÜ3,Ï:IùGE APRTT L?6"r acitro\'fT.m)Gm{msrs The ç'råter v¡Èshes to e:qpress hi s mrnest appreciatf on to Jan:ice, A.LLísou and. Davåd., Írz acknowledgenaent of thefr patÍenee anð u.nåerstaadågg ín vi.ll-iragly glvfrug 'ap thefr ri.ghts to 'the eompanS"orashåp anå at'Lentínn r¡f a husba.trð and' fether during the many hours sPent on this thesis. I&ny that:les ave alnc¡ åt¿Ë to Professor E" Ktliper for his årrspåratiou in the i,nitåatlon of, this stud-y and' his guldance ancl assåstanee tÏ.lz"oughout " The w.riter would also Like to eryrers his appreciation to the månage¡geni and ,sf"aff af Underwooð, Mçtellan and. AssocÍates, for their ånteres'L a.rio Ínvolvement ån thj"s thesis, especially to Meser"s" A. G. Spaffor"d" and R. c. La'tta, vå'bhout whose gtrÍdance and assÍstance this thesís j..n j"ts fånãt fow¡r wou[d. t ot be possfble' The r+¡"íter also wÍshes to acknovf-ed-ge grateful-Ly the assfs.tance of 3,fr. -
Lake Manitoba and Lake St. Martin Outlet Channels
Project Description Lake Manitoba and Lake St. Martin Outlet Channels Prepared for: Canadian Environmental Assessment Agency Submitted by: Manitoba Infrastructure January 2018 Project Description – January 2018 Table of Contents 1 GENERAL INFORMATION AND CONTACTS ................................................... 1 1.1 Nature of the Project and Proposed Location ..................................................... 1 1.2 Proponent Information ........................................................................................ 3 1.2.1 Name of the Project ......................................................................................... 3 1.2.2 Name of the Proponent ................................................................................... 3 1.2.3 Address of the Proponent ................................................................................ 3 1.2.4 Chief Executive Officer .................................................................................... 3 1.2.5 Principal Contact Person ................................................................................. 3 1.3 Jurisdictions and Other Parties Consulted .......................................................... 6 1.4 Environmental Assessment Requirements ......................................................... 7 1.4.1 Canadian Environmental Assessment Act, 2012 (Canada) ............................ 7 1.4.2 The Environment Act (Manitoba) ..................................................................... 8 1.5 Other Regulatory Requirements ........................................................................ -
Manitoba Lake Wind Effect Forecast for May 6 AM, 2021 Ü
Manitoba Lake Wind Effect Forecast for May 6 AM, 2021 Ü Winnipegosis !P Dauphin Lake Steep Rock !P !P Ochre Beach !P Victoria Lundar Beach Beach !P !P Gimli !P Sandy Bay !P Twin Lakes Beach !P Lynchs Point !P Oak Lake Beach !P 1:220,000 1:1,500,000 Ave.Dir.from Ave. Speed Ave.Dir.from Ave. Speed Wind Effect Alert Categories Location North (degree) (km/h) Location North (degree) (km/h) Crest level increase will be greater than 1.5 meters; Dauphin Lake NW (320) 21 Manipogo area NW (336) 15 Severe MB Lake west side - Sandy Bay W (292) 18 Crane River area NW (335) 12 Wave action will be very significant and forceful. MB Lake south side - Twin Beaches W (274) 17 Wpg Lake - Victoria Beach W (289) 12 Crest level increase will be in a range 0.9 ~ 1.5 meters; High MB Lake middle - Vogar/The Narrows NW (311) 12 Wpg Lake - Gimli Beach NW (318) 13 Wave action will be significant. MB Lake east side - Lundar Beach W (281) 12 Wpg Lake - Alberta Beach NW (293) 11 Crest level increase will be in a range 0.6 ~ 0.9 meters; Northend 1 N (351) 9 Wpg Lake - O'Hanly W (292) 11 Moderate-High Northend 2 N (344) 11 Wpg Lake south side NW (294) 11 Wave action will be considerable. Guynemer NW (337) 12 Lake Winnipegosis south side N (343) 19 Crest level increase will be in a range 0.3 ~ 0.6 meters; Moderate The Bluff NW (331) 14 Oak Lake east side community W (276) 18 Wave action will be moderate. -
Portage Diversion Layout Recent and Future Projects
Portage Diversion Layout Recent and Future Projects Assiniboine River Control Structure Public and worker safety improvements Completed in 2015 Works include fencing, signage, and safety boom Electrical and mechanical upgrades Ongoing Works include upgrades to 600V electrical distribution system, replacement of gate control system and mo- tor control center, new bulkhead gate hoist, new stand-by diesel generator fuel/piping system and new ex- terior diesel generator Portage Diversion East Outside Drain Reconstruction of 18 km of drain Completed in 2013 Replacement of culverts beneath three (3) railway crossings Completed in 2018 Recent and Future Projects Portage Diversion Outlet Structure Construction of temporary rock apron to stabilize outlet structure Completed in 2018 Conceptual Design for options to repair or replace structure Completed in 2018 Outlet structure major repair or replacement prioritized over next few years Portage Diversion Channel Removal of sedimentation within channel Completed in 2017 Groundwater/soil salinity study for the Portage Diversion Ongoing—commenced in 2016 Enhancement of East Dike north of PR 227 to address freeboard is- sues at design capacity of 25,000 cfs Proposed to commence in 2018 Multi-phase over the next couple of years Failsafe assessment and potential enhancement of West Dike to han- dle design capacity of 25,000 cfs Prioritized for future years—yet to be approved Historical Operating Guidelines Portage Diversion Operating Guidelines 1984 Red River Floodway Program of Operation Operation Objectives The Portage Diversion will be operated to meet these objectives: 1. To provide maximum benefits to the City of Winnipeg and areas along the Assiniboine River downstream of Portage la Prairie. -
CHARACTERISTICS and DISTRIBUTION of LAKES 631 Lake Winnipegosis, Lying to the North of Lake Manitoba
CHARACTERISTICS AND DISTRIBUTION OF LAKES 631 Lake Winnipegosis, lying to the north of Lake Manitoba. at an elevation of 828 feet above sea-level, is about 130 miles long, by 20 miles in maximum breadth. It covers an area of 2080 square miles, and has a maximum depth of 38 feet. It is fed by many small streams from the west, and by the overflow of Lake Dauphin (840 feet above sea-level) through Mossy River. The outlet is by the very indirect way of Waterhen River, through Waterhen Lake, to Lake Manitoba. The total area of the lakes in the Winnipeg basin is 13,500 square miles. Lake Wollaston, 1300 feet above sea-level, is the ultimate source River of the Reindeer River, one of the chief tributaries of the Churchill Churchill. River. It is about 800 square miles in area, and discharges by two outlets—to the north by the Stone River into the extreme eastern arm of Lake Athabasca, and to the south-east by the Cochrane River into Reindeer Lake. Reindeer Lake, 1150 feet above sea-level, is 135 miles long, and has an area of 2490 square miles; the Reindeer River carries its overflow to the Churchill River. The rivers in Labrador are often like strings of lakes, and divide River Rupert. and unite again in their course, while the lakes frequently discharge in two directions. Lake Mistassini, 1350 feet above sea-level, the largest lake, is practically two parallel lakes divided by a range of islands in the centre. The western lake is 90 miles long by 13 to 17 miles wide, and the eastern lake is 60 miles long by 5 to 10 miles wide, the greatest depths being 300 to 400 feet. -
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Photo: Thomas Fricke L % 45 5 65-#)&*.789:5* 65-#)0 .7(: ; " henever the University of Mani- The department of geological sciences, the are touched by it every day,” Elias says. “Hu- toba starts a new building project oldest of its kind in Western Canada, has mans rely on natural resources and the Earth on campus it piques Bill Brisbin’s been uncovering history in Manitoba for the is the supplier.” curiosity. What’s being constructed is of less past century. And it is celebrating its centen- He notes that geology also offers insights interest to the geology professor emeritus ary with a number of alumni events and pro- into climate change because it shows what than what the excavation uncovers – a slice jects. has happened in the past. of Manitoba’s history. Fundraising continues for two permanent “Geology is a fundamental in the world we Brisbin says when crews dug the ground for commemorative displays: a Mosaic Map of live in,” says Prof. Jim Teller. He points out the new lecture theatre at St. John’s College Manitoba to showcase the province’s ma- that where people spend their vacations, in 2008, it exposed clay deposits that had jor geological terrains in actual rock, and a where farmers grow their crops, the resour- been scoured off a retreating ice sheet about 5.5-metre History Wall to chronicle the de- ces that are mined, and even the landscapes 10,000 years ago. partment’s history, achievements, alumni of that photographers decide to shoot are all de- But you don’t have to dig deep to go even distinction and academic and professional termined by geology. -
RIVERS and LAKES 11 the Great Lakes.—Table 4 Shows the Length
RIVERS AND LAKES 11 The Great Lakes.—Table 4 shows the length, breadth, area, elevation above sea-level and maximum depth of each of the Great Lakes. i.—Area, Elevation and Depth of the Great Lakes. Maximum Elevation Lakes. Length. Breadth. depth. Area. above sea-level. square miles. miles. feet. miles. feet. Superior... 383 160 1,180 31,810 602-29 Michigan.. 320 118 870 22,400 581-13 Huron 247 101 750 23,010 581-13 St. Clair.., 26 24 23 460 575-62 Erie 241 57 210 9,940 572-52 Ontario 180 53 738 7,540 246-17 Lake Superior, with its area of 31,810 square miles, is the largest body of fresh water in the world. As the international boundary between Canada and the United States passes through the centre of lakes Superior, Huron, Erie, St. Clair and Ontario, only half of the areas of these lakes given in the above statement is Canadian. The whole of lake Michigan is within United States territory. From the western end of lake Superior to the mouth of the St. Lawrence there is, with the aid of the canal system, a continuous navigable waterway. The total length of the St. Law rence river from the head of the St. Louis river to Pointe-des-Monts, at the entrance of the gulf of St. Lawrence, is 1,900 miles. The tributaries of the St. Lawrence, several of which have themselves important tributaries, include the Ottawa river, 685 miles long, the St. Maurice river, 325 miles long, and the Sague- nay (to head of Peribonka), 405 miles long.